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,{"id":28411,"text":"wri874103 - 1987 - Ground-water resources of the Bisbee-Naco Area, Cochise County, Arizona","interactions":[],"lastModifiedDate":"2012-02-02T00:08:50","indexId":"wri874103","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"87-4103","title":"Ground-water resources of the Bisbee-Naco Area, Cochise County, Arizona","docAbstract":"The Bisbee-Naco Area is in southeastern Arizona and northeastern Sonora, Mexico. Annual rainfall averages about 17 inches. The basin fill is the principal aquifer and supplies about 95% of all water for domestic purposes. The total groundwater pumped in 1985 was about 6,500 acre/ft. Of that amount, 2,200 acre-ft was used for domestic use and the rest was used for irrigation and livestock. Domestic use is expected to increase 20% by the year 2000. Water levels at the Bisbee well field have remained virtually unchanged since 1953, but water levels have declined about 25% in areas east and southeast of the well field. The native groundwater in the area is a calcium bicarbonate type and generally is suitable for domestic use. Groundwater down-gradient from a mine tailings pond contains 650 to 850 mg/l of sulfate. Recharge occurs naturally through direct infiltration or rainfall along the mountain fronts and through subsurface inflow from adjacent areas. Some water is recharged through direct infiltration from a mine tailings pond, sewage ponds, septic systems, and urban runoff. The potential for contamination exists from mine tailings, sewage, and urban runoff. No other sources of drinking water are readily available in the immediate area. Potential alternate sources of drinking water are the aquifers underlying Sulphur Spring Valley and San Pedro River valley. (Author 's abstract)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri874103","usgsCitation":"Littin, G.R., 1987, Ground-water resources of the Bisbee-Naco Area, Cochise County, Arizona: U.S. Geological Survey Water-Resources Investigations Report 87-4103, iv, 34 p. :ill., map ;28 cm., https://doi.org/10.3133/wri874103.","productDescription":"iv, 34 p. :ill., map ;28 cm.","costCenters":[],"links":[{"id":122696,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1987/4103/report-thumb.jpg"},{"id":57215,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1987/4103/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afde4b07f02db696baf","contributors":{"authors":[{"text":"Littin, G. R.","contributorId":95924,"corporation":false,"usgs":true,"family":"Littin","given":"G.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":199751,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":30213,"text":"wri874013 - 1987 - Potential for pollution of the Upper Floridan aquifer from five sinkholes and an internally drained basin in west-central Florida","interactions":[],"lastModifiedDate":"2012-02-02T00:08:50","indexId":"wri874013","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"87-4013","title":"Potential for pollution of the Upper Floridan aquifer from five sinkholes and an internally drained basin in west-central Florida","docAbstract":"Sinkholes are natural and common geologic features in west-central Florida, which is underlain by water soluble limestone deposits. Dissolution of these deposits is the fundamental cause of sinkhole development. Sinkholes and other karst features are more pronounced in the northern part of the study area, but sinkhole activity has occurred throughout the area. Fifty-eight sinkholes with known or suspected connection to the Upper Floridan aquifer are located in the study area. An internally drained basin near the city of Brandon and five sinkholes in Hillsborough, Pasco, and Hernando Counties were selected for detailed investigation. At all sites, chemical or biological constituents were detected that indicate pollutants had entered the aquifer. A generalized classification, based on the potential to pollute, was applied to the selected sites. Four of the sites have high potential and two have moderate potential to pollute the Upper Floridan aquifer. All of the sites investigated are capable of recharging large volumes of water to the Upper Floridan aquifer in short periods of time. Continued monitoring of the quality of water entering the sinkholes and of wells downgradient to the sinks is needed to assess the future impacts on the aquifer. (Author 's abstract)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri874013","usgsCitation":"Trommer, J., 1987, Potential for pollution of the Upper Floridan aquifer from five sinkholes and an internally drained basin in west-central Florida: U.S. Geological Survey Water-Resources Investigations Report 87-4013, vii, 103 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri874013.","productDescription":"vii, 103 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":124010,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1987/4013/report-thumb.jpg"},{"id":59000,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1987/4013/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad5e4b07f02db6835ee","contributors":{"authors":[{"text":"Trommer, J.T.","contributorId":28248,"corporation":false,"usgs":true,"family":"Trommer","given":"J.T.","email":"","affiliations":[],"preferred":false,"id":202868,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":26719,"text":"wri874207 - 1987 - Technique for estimating flood-peak discharges and frequencies on rural streams in Illinois","interactions":[],"lastModifiedDate":"2012-02-02T00:08:30","indexId":"wri874207","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"87-4207","title":"Technique for estimating flood-peak discharges and frequencies on rural streams in Illinois","docAbstract":"Flood-peak discharges and frequencies are presented for 394 gaged sites in Illinois, Indiana, and Wisconsin for recurrence intervals ranging from 2 to 100 years. A technique is presented for estimating flood-peak discharges at recurrence intervals ranging from 2 to 500 years for nonregulated streams in Illinois with drainage areas ranging from 0.02 to 10,000 square miles. Multiple-regression analyses, using basin characteristics and peak streamflow data from 268 of the 394 gaged sites, were used to define the flood-frequency relation. The most significant independent variables for estimating flood-peak discharge are drainage area, slope, rainfall intensity and a regional factor. Examples are given to show a step-by-step procedure in calculating a 50-year flood for a site on an ungaged stream, a site at a gaged location, and a site near a gaged location. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri874207","usgsCitation":"Curtis, G., 1987, Technique for estimating flood-peak discharges and frequencies on rural streams in Illinois: U.S. Geological Survey Water-Resources Investigations Report 87-4207, v, 79 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri874207.","productDescription":"v, 79 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":2054,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://il.water.usgs.gov/pubsearch/reports.cgi/view?series=WRIR&number=87-4207","linkFileType":{"id":5,"text":"html"}},{"id":158251,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1987/4207/report-thumb.jpg"},{"id":55593,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1987/4207/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adce4b07f02db6862d3","contributors":{"authors":[{"text":"Curtis, G.W.","contributorId":69159,"corporation":false,"usgs":true,"family":"Curtis","given":"G.W.","email":"","affiliations":[],"preferred":false,"id":196884,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":26688,"text":"wri864208 - 1987 - Streamflow and water quality of the Grand Calumet River, Lake County, Indiana, and Cook County, Illinois, October 1984","interactions":[],"lastModifiedDate":"2016-06-01T16:20:46","indexId":"wri864208","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"86-4208","title":"Streamflow and water quality of the Grand Calumet River, Lake County, Indiana, and Cook County, Illinois, October 1984","docAbstract":"<p>A diel (24-hour) water-quality survey was done to investigate the sources of dry-weather waste inputs attributable to other than permitted point-source effluent and to evaluate the waste-load assimilative capacity of the Grand Calumet River, Lake County, Indiana, and Cook County, Illinois, in October 1984. Flow in the Grand Calumet River consists almost entirely of municipal and industrial effluents which comprised more than 90% of the 500 cu ft/sec flow observed at the confluence of the East Branch Grand Calumet River and the Indiana Harbor Ship Canal during the study. At the time of the study, virtually all of the flow in the West Branch Grand Calumet River was municipal effluent. Diel variations in streamflow of as much as 300 cu ft/sec were observed in the East Branch near the ship canal. The diel variation diminished at the upstream sampling sites in the East Branch. In the West Branch, the diel variation in flow was quite drastic; complete reversals of flow were observed at sampling stations near the ship canal. Average dissolved-oxygen concentrations at stations in the East Branch ranged from 5.7 to 8.2 mg/L and at stations in the West Branch from 0.8 to 6.6 mg/L. Concentrations of dissolved solids, suspended solids, biochemical-oxygen demand, ammonia, nitrite, nitrate, and phosphorus were substantially higher in the West Branch than in the East Branch. In the East Branch, only the Indiana Stream Pollution Control Board water-quality standards for total phosphorus and phenol were exceeded. In the West Branch, water-quality standards for total ammonia, chloride, cyanide, dissolved solids, fluoride, total phosphorus, mercury, and phenol were exceeded and dissolved oxygen was less than the minimum allowable. Three areas of significant differences between cumulative effluent and instream chemical-mass discharges were identified in the East Branch and one in the West Branch. The presence of unidentified waste inputs in the East Branch were indicated by differences in the chemical-mass discharges at three sites. Elevated suspended solids, biochemical-oxygen demand, and ammonia chemical-mass discharges at Columbia Avenue indicated the presence of a source of what may have been untreated sewage to the West Branch during the survey. (Author 's abstract)</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Indianapolis, IN","doi":"10.3133/wri864208","collaboration":"Prepared in cooperation with the Indiana State Board of Health","usgsCitation":"Crawford, C.G., and Wangsness, D.J., 1987, Streamflow and water quality of the Grand Calumet River, Lake County, Indiana, and Cook County, Illinois, October 1984: U.S. Geological Survey Water-Resources Investigations Report 86-4208, xi, 137 p., https://doi.org/10.3133/wri864208.","productDescription":"xi, 137 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":346,"text":"Indiana Water Science Center","active":true,"usgs":true}],"links":[{"id":158852,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1986/4208/report-thumb.jpg"},{"id":55551,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1986/4208/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United 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Charles G. 0000-0003-1653-7841 cgcrawfo@usgs.gov","orcid":"https://orcid.org/0000-0003-1653-7841","contributorId":1064,"corporation":false,"usgs":true,"family":"Crawford","given":"Charles","email":"cgcrawfo@usgs.gov","middleInitial":"G.","affiliations":[{"id":37947,"text":"Upper Midwest Water Science Center","active":true,"usgs":true},{"id":451,"text":"National Water Quality Assessment Program","active":true,"usgs":true}],"preferred":true,"id":196832,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wangsness, David J.","contributorId":81475,"corporation":false,"usgs":true,"family":"Wangsness","given":"David","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":196833,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":80290,"text":"fwsobs82_10_138 - 1987 - Habitat Suitability Index Models: Bullfrog","interactions":[],"lastModifiedDate":"2022-01-28T17:54:10.782857","indexId":"fwsobs82_10_138","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":20,"text":"FWS/OBS","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"82/10.138","subseriesTitle":"Habitat Suitability Index","title":"Habitat Suitability Index Models: Bullfrog","docAbstract":"A review and synthesis of existing information were used to develop a Habitat Suitability Index (HSI) model for the bullfrog (Rana catesbeiana). The model consolidates habitat use information into a framework appropriate for field application, and is scaled to produce an index between 0.0 (unsuitable habitat) to 1.0 (optimum habitat). HSI models are designed to be used with Habitat Evaluation Procedures previously developed by the U.S. Fish and Wildlife Service.","language":"English","publisher":"U.S. Fish and Wildlife Service","usgsCitation":"Graves, B.M., and Anderson, S.H., 1987, Habitat Suitability Index Models: Bullfrog: FWS/OBS 82/10.138, viii, 22 p.","productDescription":"viii, 22 p.","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":195611,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aeee4b07f02db6912f6","contributors":{"authors":[{"text":"Graves, Brent M.","contributorId":101338,"corporation":false,"usgs":true,"family":"Graves","given":"Brent","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":292189,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Anderson, Stanley H.","contributorId":68361,"corporation":false,"usgs":true,"family":"Anderson","given":"Stanley","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":292188,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":36221,"text":"b1802 - 1987 - Evaluating coinciding anomalies along a fault trace or other traverse; simulations and statistical procedures","interactions":[],"lastModifiedDate":"2012-02-02T00:09:41","indexId":"b1802","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":306,"text":"Bulletin","code":"B","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1802","title":"Evaluating coinciding anomalies along a fault trace or other traverse; simulations and statistical procedures","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/b1802","usgsCitation":"Wheeler, R.L., and Krystinik, K.B., 1987, Evaluating coinciding anomalies along a fault trace or other traverse; simulations and statistical procedures: U.S. Geological Survey Bulletin 1802, iii, 12 p. :ill., map ;28 cm., https://doi.org/10.3133/b1802.","productDescription":"iii, 12 p. :ill., map ;28 cm.","costCenters":[],"links":[{"id":166591,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1802/report-thumb.jpg"},{"id":64169,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1802/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a09e4b07f02db5fb0d4","contributors":{"authors":[{"text":"Wheeler, Russell L. wheeler@usgs.gov","contributorId":858,"corporation":false,"usgs":true,"family":"Wheeler","given":"Russell","email":"wheeler@usgs.gov","middleInitial":"L.","affiliations":[],"preferred":false,"id":215969,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Krystinik, Katherine B.","contributorId":77989,"corporation":false,"usgs":true,"family":"Krystinik","given":"Katherine","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":215970,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":4341,"text":"cir1008 - 1987 - Landslides of Eastern North America","interactions":[{"subject":{"id":70189595,"text":"cir10084 - 1987 - Preliminary results from a study of natural slope failures triggered by the storm of November 3.5.1985, Germany Valley, West Virginia and Virginia: Chapter 4 in Landslides of eastern North America","indexId":"cir10084","publicationYear":"1987","noYear":false,"chapter":"4","displayTitle":"Preliminary results from a study of natural slope failures triggered by the storm of November 3.5.1985, Germany Valley, West Virginia and Virginia: Chapter 4 in <i>Landslides of eastern North America</i>","title":"Preliminary results from a study of natural slope failures triggered by the storm of November 3.5.1985, Germany Valley, West Virginia and Virginia: Chapter 4 in Landslides of eastern North America"},"predicate":"IS_PART_OF","object":{"id":4341,"text":"cir1008 - 1987 - Landslides of Eastern North America","indexId":"cir1008","publicationYear":"1987","noYear":false,"title":"Landslides of Eastern North America"},"id":1}],"lastModifiedDate":"2012-02-02T00:05:34","indexId":"cir1008","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"1008","title":"Landslides of Eastern North America","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/cir1008","usgsCitation":"Schultz, A.P., and Southworth, C., 1987, Landslides of Eastern North America: U.S. Geological Survey Circular 1008, vii, 43 p. :ill., maps ;28 cm., https://doi.org/10.3133/cir1008.","productDescription":"vii, 43 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":117336,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1987/1008/report-thumb.jpg"},{"id":31451,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1987/1008/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1be4b07f02db6a9199","contributors":{"authors":[{"text":"Schultz, Arthur P. aschultz@usgs.gov","contributorId":3252,"corporation":false,"usgs":true,"family":"Schultz","given":"Arthur","email":"aschultz@usgs.gov","middleInitial":"P.","affiliations":[{"id":243,"text":"Eastern Geology and Paleoclimate Science Center","active":true,"usgs":true}],"preferred":true,"id":148880,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Southworth, C.S.","contributorId":51272,"corporation":false,"usgs":true,"family":"Southworth","given":"C.S.","email":"","affiliations":[],"preferred":false,"id":148881,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":28647,"text":"wri874030 - 1987 - Movement and fate of ethylene dibromide (EDB) in ground water in Seminole County, Georgia","interactions":[],"lastModifiedDate":"2017-01-24T12:51:54","indexId":"wri874030","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"87-4030","title":"Movement and fate of ethylene dibromide (EDB) in ground water in Seminole County, Georgia","docAbstract":"An investigation to assess the movement and fate of ethylene dibromide (EDB) in the Upper Floridan aquifer (formerly the principal artesian aquifer) was conducted, because a previous investigation conducted in August 1983, had found EDB contamination of the aquifer in about a 4 sq mi area in central Seminole County, Georgia. Analyses of water from wells resampled in June 1985 indicate that EDB was present in the groundwater 2 yr after last being applied as a soil fumigant. The investigation revealed that groundwater recharge and irrigation pumping between August 1983 and June 1985 did not substantially change the areal extent of EDB in the Upper Floridan aquifer but concentrations of EDB seem to be declining. The highest concentrations again were found in two irrigation wells near Buck Hole, a sinkhole in a swampy depression in central Seminole County. EDB concentrations in these two wells ranged from 1.5 to 13 micrograms/L. Samples from two of three wells in the residuum near Buck Hole also had detectable concentrations of EDB. The presence of EDB in water samples from wells tapping the residuum and wells tapping the Upper Floridan aquifer indicates that agriculturally applied EDB has moved downward from the surface soils through the residuum and into the aquifer. Results of aquifer tests conducted in a similar geohydrologic setting suggest that local pumping from the highly transmissive aquifer may accelerate downward movement of water and EDB. Potentiometric surface maps of the Upper Floridan aquifer indicate that east of Fishpond Drain, where the highest concentrations of EDB were detected, the direction of groundwater flow and the direction of potential EDB transport generally is south-southeasterly. However, the movement of an EDB plume from the area of relatively high concentrations near Buck Hole along inferred groundwater flow lines was not detected. (Author 's abstract)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri874030","usgsCitation":"McConnell, J.B., 1987, Movement and fate of ethylene dibromide (EDB) in ground water in Seminole County, Georgia: U.S. Geological Survey Water-Resources Investigations Report 87-4030, v, 13 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri874030.","productDescription":"v, 13 p. :ill., maps ;28 cm.","costCenters":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"links":[{"id":123785,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1987/4030/report-thumb.jpg"},{"id":57491,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1987/4030/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Georgia","county":"Seminole County","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -84.649658203125,\n              30.873940237887624\n            ],\n            [\n              -84.737548828125,\n              30.770159115784214\n            ],\n            [\n              -84.847412109375,\n              30.694611546632277\n            ],\n            [\n              -84.935302734375,\n              30.770159115784214\n            ],\n            [\n              -84.957275390625,\n              30.911651004518244\n            ],\n            [\n              -85.001220703125,\n              31.052933985705163\n            ],\n            [\n              -85.111083984375,\n              31.175209828310845\n            ],\n            [\n              -84.627685546875,\n              31.175209828310845\n            ],\n            [\n              -84.649658203125,\n              30.873940237887624\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b32e4b07f02db6b47f8","contributors":{"authors":[{"text":"McConnell, J. B.","contributorId":25577,"corporation":false,"usgs":true,"family":"McConnell","given":"J.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":200168,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":28649,"text":"wri844158 - 1987 - Simulated flood discharges and elevations for the Savannah River, South Carolina and Georgia, using an unsteady streamflow model","interactions":[],"lastModifiedDate":"2017-01-24T09:57:11","indexId":"wri844158","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"84-4158","title":"Simulated flood discharges and elevations for the Savannah River, South Carolina and Georgia, using an unsteady streamflow model","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri844158","usgsCitation":"McDonald, B., and Sanders, C., 1987, Simulated flood discharges and elevations for the Savannah River, South Carolina and Georgia, using an unsteady streamflow model: U.S. Geological Survey Water-Resources Investigations Report 84-4158, 34 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri844158.","productDescription":"34 p. :ill., maps ;28 cm.","costCenters":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"links":[{"id":158841,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1984/4158/report-thumb.jpg"},{"id":57492,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1984/4158/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Georgia, South Carolina","otherGeospatial":"Savannah River","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {\n        \"stroke\": \"#555555\",\n        \"stroke-width\": 2,\n        \"stroke-opacity\": 1,\n        \"fill\": \"#555555\",\n        \"fill-opacity\": 0.5\n      },\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -83.133544921875,\n              34.1890858311724\n            ],\n            [\n              -82.7984619140625,\n              34.347971491244955\n            ],\n            [\n              -82.50732421875,\n              34.39331222316112\n            ],\n            [\n              -80.9857177734375,\n              32.54218257955074\n            ],\n            [\n              -81.617431640625,\n              32.21280106801518\n            ],\n            [\n              -83.133544921875,\n              34.1890858311724\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f9e4b07f02db5f3316","contributors":{"authors":[{"text":"McDonald, B.B.","contributorId":44551,"corporation":false,"usgs":true,"family":"McDonald","given":"B.B.","email":"","affiliations":[],"preferred":false,"id":200171,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sanders, C.L.","contributorId":41001,"corporation":false,"usgs":true,"family":"Sanders","given":"C.L.","affiliations":[],"preferred":false,"id":200170,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":28857,"text":"wri864335 - 1987 - Magnitude and frequency of floods in Arkansas","interactions":[],"lastModifiedDate":"2012-02-02T00:08:44","indexId":"wri864335","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"86-4335","title":"Magnitude and frequency of floods in Arkansas","docAbstract":"The magnitude and frequency of peak discharges on streams in Arkansas, were estimated through the use of comprehensive regression analyses, in which physical characteristics of streams were related to flood characteristics at gaging stations. Equations derived from the regression analyses provide estimates of peak discharges with selected recurrence intervals from 2 to 100 yrs on streams that have drainage areas &lt; 3,000 sq mi. The regression analyses indicate that size of drainage area, slope of the main channel, length of the main channel, elevation of the basin, and mean annual precipitation were the most significant basin and climatic characteristics that affect the magnitude and frequency of floods. A technique is presented for estimating a stage-discharge relation at ungaged sites based on a cross section determined from topographic maps. This cross-section and stage-discharge relation is then used to determine the hydraulic radius for the discharges at each recurrence interval. Techniques are presented for estimating the magnitude and frequency of peak discharges using the hydraulic radius with other physical characteristics of the basin. The techniques that use the hydraulic radius give standard errors of estimate from 5% to 16% lower than techniques that do not use hydraulic radius. Data from 200 gaging stations with drainage areas less than 3,000 sq mi and with at least 10 yrs of record were used in the analyses. Large rivers such as the Red, Arkansas, White, Black, St. Francis, Mississippi, and Ouachita Rivers have flood flow characteristics that differ from those of smaller tributary streams and were, therefore, treated individually. Regional regression equations are not applicable to the large rivers; the magnitude and frequency of floods along these rivers are based on station data. A method is described for estimating the magnitude and frequency of peak discharges on streams for urban areas in Arkansas. (Lantz-PTT)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri864335","usgsCitation":"Neely, B., 1987, Magnitude and frequency of floods in Arkansas: U.S. Geological Survey Water-Resources Investigations Report 86-4335, v, 51 p. :maps ;28 cm., https://doi.org/10.3133/wri864335.","productDescription":"v, 51 p. :maps ;28 cm.","costCenters":[],"links":[{"id":124291,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1986/4335/report-thumb.jpg"},{"id":57728,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1986/4335/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a80e4b07f02db649544","contributors":{"authors":[{"text":"Neely, B.L.","contributorId":90344,"corporation":false,"usgs":true,"family":"Neely","given":"B.L.","affiliations":[],"preferred":false,"id":200514,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":64103,"text":"gp970 - 1987 - Free-air gravity anomaly map of the Umnak Plateau region, southeastern Bering Sea","interactions":[],"lastModifiedDate":"2012-02-10T00:10:56","indexId":"gp970","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":317,"text":"Geophysical Investigations Map","code":"GP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"970","title":"Free-air gravity anomaly map of the Umnak Plateau region, southeastern Bering Sea","language":"ENGLISH","doi":"10.3133/gp970","usgsCitation":"Childs, J., Magistrale, H., and Cooper, A.K., 1987, Free-air gravity anomaly map of the Umnak Plateau region, southeastern Bering Sea: U.S. Geological Survey Geophysical Investigations Map 970, 1 map :col. ;67 x 83 cm., on sheet 81 x 112 cm., folded in envelope 25 x 32 cm., https://doi.org/10.3133/gp970.","productDescription":"1 map :col. ;67 x 83 cm., on sheet 81 x 112 cm., folded in envelope 25 x 32 cm.","costCenters":[],"links":[{"id":105389,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_6312.htm","linkFileType":{"id":5,"text":"html"},"description":"6312"},{"id":187196,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"1000000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -174,52 ], [ -174,58 ], [ -16.333333333333332,58 ], [ -16.333333333333332,52 ], [ -174,52 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1ae4b07f02db6a86d6","contributors":{"authors":[{"text":"Childs, J.R.","contributorId":63011,"corporation":false,"usgs":true,"family":"Childs","given":"J.R.","email":"","affiliations":[],"preferred":false,"id":269953,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Magistrale, H.W.","contributorId":6137,"corporation":false,"usgs":true,"family":"Magistrale","given":"H.W.","email":"","affiliations":[],"preferred":false,"id":269951,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Cooper, A. K.","contributorId":50149,"corporation":false,"usgs":true,"family":"Cooper","given":"A.","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":269952,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":28847,"text":"wri874021 - 1987 - Ground-water resources of Flagler County, Florida","interactions":[],"lastModifiedDate":"2012-02-02T00:08:44","indexId":"wri874021","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"87-4021","title":"Ground-water resources of Flagler County, Florida","docAbstract":"Groundwater is the only significant source of potable water in Flagler County. Usable water occurs in the Upper Floridan aquifer, the intermediate population is expected to place stresses on the water resources of the county. Although rainfall averages almost 50 in/yr, most of the water leaves as evapotranspiration and streamflow. Less than 1 in/yr recharge may be occurring to the Upper Floridan aquifer, the highest yielding aquifer. The Upper Floridan aquifer consists of the Avon Park Formation, the Ocala Limestone, and the basal dolomitic limestone of the Hawthorne. Use of the Upper Floridan aquifer for public water supply is limited in most of the county because it contains marginally potable or brackish water. It is used extensively for agricultural irrigation. The intermediate aquifer system consists of thin, discontinues lenses of sand, shell, and limestone between clays overlying the Floridan aquifer system. The intermediate aquifer system is an important part of the public water supply of the county because of the good quality of the water. The intermediate aquifer system has variable yields because of the discontinuous lenses. The surficial aquifer system is composed of sand and shell with varying fractions of finer materials. Well yields are small in the west and central parts of Flagler County, but the surficial aquifer system is an adequate source of domestic supply on the barrier island. A zone of freshwater in the surficial aquifer system is very important in the Hammock area, being the local source of most domestic supply in the area. Changes in hydrologic conditions from the 1950 's include a long-term decline in water levels in the Upper Floridan aquifer coincident with lower-than-average rainfall and a greater seasonal fluctuation of water levels. Chloride concentrations of water in the Upper Floridan aquifer do not appear to have changed significantly, presently ranging from 7 to 3,700 mg/L. Development will place stress on the aquifers and may result in upconing of brackish water in pumping centers and in lateral saltwater intrusion in coastal areas. (Author 's abstract)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri874021","usgsCitation":"Navoy, A., and Bradner, L.A., 1987, Ground-water resources of Flagler County, Florida: U.S. Geological Survey Water-Resources Investigations Report 87-4021, v, 45 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri874021.","productDescription":"v, 45 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":123701,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1987/4021/report-thumb.jpg"},{"id":57720,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1987/4021/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a6be4b07f02db63d2c8","contributors":{"authors":[{"text":"Navoy, A. S.","contributorId":51771,"corporation":false,"usgs":true,"family":"Navoy","given":"A. S.","affiliations":[],"preferred":false,"id":200501,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bradner, L. A.","contributorId":21925,"corporation":false,"usgs":true,"family":"Bradner","given":"L.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":200500,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":61390,"text":"mf1244C - 1987 - Aeromagnetic map of the Mt. Moriah Roadless Area, White Pine County, Nevada","interactions":[],"lastModifiedDate":"2019-05-28T15:55:03","indexId":"mf1244C","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":325,"text":"Miscellaneous Field Studies Map","code":"MF","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1244","chapter":"C","title":"Aeromagnetic map of the Mt. Moriah Roadless Area, White Pine County, Nevada","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/mf1244C","isbn":"0607807776","usgsCitation":"Martin, R., 1987, Aeromagnetic map of the Mt. Moriah Roadless Area, White Pine County, Nevada: U.S. Geological Survey Miscellaneous Field Studies Map 1244, 1 Plate: 42 x 39 cm., https://doi.org/10.3133/mf1244C.","productDescription":"1 Plate: 42 x 39 cm.","costCenters":[],"links":[{"id":364213,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1244-C/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":183463,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/mf/1244-C/report-thumb.jpg"}],"scale":"62500","country":"United States","state":"Nevada","county":"White Pine County","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -114.33333333333333,39.134166666666665 ], [ -114.33333333333333,39.3675 ], [ -114.0675,39.3675 ], [ -114.0675,39.134166666666665 ], [ -114.33333333333333,39.134166666666665 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4af4e4b07f02db691d38","contributors":{"authors":[{"text":"Martin, R.A.","contributorId":53379,"corporation":false,"usgs":true,"family":"Martin","given":"R.A.","email":"","affiliations":[],"preferred":false,"id":265564,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":38500,"text":"pp1384 - 1987 - Flow model for open-channel reach or network","interactions":[],"lastModifiedDate":"2012-02-02T00:10:20","indexId":"pp1384","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"1384","title":"Flow model for open-channel reach or network","docAbstract":"Formulation of a one-dimensional model for simulating unsteady flow in a single open-channel reach or in a network of interconnected channels is presented. The model is both general and flexible in that it can be used to simulate a wide range of flow conditions for various channel configurations. It is based on a four-point (box), implicit, finite-difference approximation of the governing nonlinear flow equations with user-definable weighting coefficients to permit varying the solution scheme from box-centered to fully forward. Unique transformation equations are formulated that permit correlation of the unknowns at the extremities of the channels, thereby reducing coefficient matrix and execution time requirements. Discharges and water-surface elevations computed at intermediate locations within a channel are determined following solution of the transformation equations. The matrix of transformation and boundary-condition equations is solved by Gauss elimination using maximum pivot strategy. Two diverse applications of the model are presented to illustrate its broad utility. (USGS)","language":"ENGLISH","doi":"10.3133/pp1384","usgsCitation":"Schaffranek, R., 1987, Flow model for open-channel reach or network: U.S. Geological Survey Professional Paper 1384, 11 p., https://doi.org/10.3133/pp1384.","productDescription":"11 p.","costCenters":[],"links":[{"id":126695,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1384/report-thumb.jpg"},{"id":65216,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1384/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49d8e4b07f02db5df252","contributors":{"authors":[{"text":"Schaffranek, R.W.","contributorId":61468,"corporation":false,"usgs":true,"family":"Schaffranek","given":"R.W.","affiliations":[],"preferred":false,"id":219943,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":29118,"text":"wri864016 - 1987 - Water quality of Fremont Lake and New Fork Lakes, western Wyoming: A progress report","interactions":[],"lastModifiedDate":"2022-12-19T20:09:14.384152","indexId":"wri864016","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"86-4016","title":"Water quality of Fremont Lake and New Fork Lakes, western Wyoming: A progress report","docAbstract":"<p>Fremont Lake and New Fork Lakes in the New Fork River drainage of western Wyoming were selected for a comprehensive study of hydrologic processes affecting mountain lakes in the Rocky Mountains. Information is needed about lakes in this area to assess their response to existing and planned development. The concerns include regional issues such as acid precipitation from gas-sweetening plants, coal-fired powerplants, and smelters, as well as local issues, such as shoreline development and raising outlet control structures. Onsite measurements indicated strong thermal stratification in the lakes during the summer. Isothermal conditions occurred during December 1983 and May 1984. Mean phytoplankton concentrations were less than 5,000 cells/ml, and chlorophyll a concentrations were weakly correlated with phytoplankton concentrations. Zooplankton concentrations were small, less than 6 organisms/L. The numbers of benthic invertebrates/unit area in Fremont Lake were extremely small. The lake waters and inflow and outflow streams were chemically dilute solutions. Mean dissolved-solids concentrations were 13 mg/L in Fremont Lake and 24 mg/L in New Fork Lakes. Calcium and bicarbonate were the predominant ions. Concentrations of phosphorus and nitrogen usually were less than detection limits. Trace-metals concentrations in the lakes were similar to those in precipitation and generally were small. Dissolved organic-carbon concentrations were about 1 mg/L. Concentrations of fulvic and humic acids were relatively large in the inlet of Fremont Lake during the spring. Pine Creek has deposited 800 metric tons of sediment, on an annual average, to the delta of Fremont Lake. Most sediment is deposited during spring runoff.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri864016","usgsCitation":"Peterson, D.A., Averett, R., and Mora, K.L., 1987, Water quality of Fremont Lake and New Fork Lakes, western Wyoming: A progress report: U.S. Geological Survey Water-Resources Investigations Report 86-4016, vi, 55 p., https://doi.org/10.3133/wri864016.","productDescription":"vi, 55 p.","costCenters":[],"links":[{"id":410729,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_36486.htm","linkFileType":{"id":5,"text":"html"}},{"id":57988,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1986/4016/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":159526,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1986/4016/report-thumb.jpg"}],"country":"United States","state":"Wyoming","otherGeospatial":"Fremont Lake and New Fork Lakes","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -109.75,\n              43.117\n            ],\n            [\n              -110,\n              43.117\n            ],\n            [\n              -110,\n              42.875\n            ],\n            [\n              -109.75,\n              42.875\n            ],\n            [\n              -109.75,\n              43.117\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a02e4b07f02db5f8110","contributors":{"authors":[{"text":"Peterson, D. A.","contributorId":6453,"corporation":false,"usgs":true,"family":"Peterson","given":"D.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":200973,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Averett, R. C.","contributorId":35709,"corporation":false,"usgs":true,"family":"Averett","given":"R. C.","affiliations":[],"preferred":false,"id":200974,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Mora, K. L.","contributorId":55008,"corporation":false,"usgs":true,"family":"Mora","given":"K.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":200975,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":38533,"text":"pp1314AL - 1987 - Geological investigations of the Vermillion Creek coal bed in the Eocene Niland Tongue of the Wasatch Formation, Sweetwater County, Wyoming","interactions":[],"lastModifiedDate":"2018-10-23T17:28:55","indexId":"pp1314AL","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"1314","chapter":"A-L","title":"Geological investigations of the Vermillion Creek coal bed in the Eocene Niland Tongue of the Wasatch Formation, Sweetwater County, Wyoming","language":"ENGLISH","doi":"10.3133/pp1314AL","usgsCitation":"Martin, P., 1987, Geological investigations of the Vermillion Creek coal bed in the Eocene Niland Tongue of the Wasatch Formation, Sweetwater County, Wyoming: U.S. Geological Survey Professional Paper 1314, iii, 202 p. : ill., maps (one col.) ; 30 cm.; 3 plates in pocket, https://doi.org/10.3133/pp1314AL.","productDescription":"iii, 202 p. : ill., maps (one col.) ; 30 cm.; 3 plates in pocket","costCenters":[],"links":[{"id":247690,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1314a-l/plate-2.pdf","size":"3615","linkFileType":{"id":1,"text":"pdf"}},{"id":247691,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1314a-l/plate-6.pdf","size":"5390","linkFileType":{"id":1,"text":"pdf"}},{"id":247689,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1314a-l/plate-1.pdf","size":"6694","linkFileType":{"id":1,"text":"pdf"}},{"id":120237,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1314a-l/report-thumb.jpg"},{"id":65296,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1314a-l/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adee4b07f02db68755a","contributors":{"editors":[{"text":"Roehler, H. W.","contributorId":16072,"corporation":false,"usgs":true,"family":"Roehler","given":"H.","middleInitial":"W.","affiliations":[],"preferred":false,"id":749488,"contributorType":{"id":2,"text":"Editors"},"rank":1}],"authors":[{"text":"Martin, P.L.","contributorId":16541,"corporation":false,"usgs":true,"family":"Martin","given":"P.L.","email":"","affiliations":[],"preferred":false,"id":220012,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":33507,"text":"b1719G - 1987 - Mineral resources of the Upper Deep Creek Wilderness Study Area, Owyhee County, Idaho","interactions":[],"lastModifiedDate":"2012-02-02T00:09:34","indexId":"b1719G","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":306,"text":"Bulletin","code":"B","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1719","chapter":"G","title":"Mineral resources of the Upper Deep Creek Wilderness Study Area, Owyhee County, Idaho","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/b1719G","usgsCitation":"Minor, S.A., King, H.D., Kulik, D.M., Sawatzky, D.L., and Capstick, D., 1987, Mineral resources of the Upper Deep Creek Wilderness Study Area, Owyhee County, Idaho: U.S. Geological Survey Bulletin 1719, v, p. G1-G14, maps (1 col.) ;28 cm., https://doi.org/10.3133/b1719G.","productDescription":"v, p. G1-G14, maps (1 col.) ;28 cm.","costCenters":[],"links":[{"id":95986,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1719g/report.pdf","size":"3716","linkFileType":{"id":1,"text":"pdf"}},{"id":166056,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1719g/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b06e4b07f02db69a019","contributors":{"authors":[{"text":"Minor, Scott A. 0000-0002-6976-9235 sminor@usgs.gov","orcid":"https://orcid.org/0000-0002-6976-9235","contributorId":765,"corporation":false,"usgs":true,"family":"Minor","given":"Scott","email":"sminor@usgs.gov","middleInitial":"A.","affiliations":[{"id":318,"text":"Geosciences and Environmental Change Science Center","active":true,"usgs":true}],"preferred":true,"id":211415,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"King, H. D.","contributorId":89113,"corporation":false,"usgs":true,"family":"King","given":"H.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":211419,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Kulik, D. M.","contributorId":46948,"corporation":false,"usgs":true,"family":"Kulik","given":"D.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":211416,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Sawatzky, D. L.","contributorId":79113,"corporation":false,"usgs":true,"family":"Sawatzky","given":"D.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":211417,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Capstick, D.O.","contributorId":79469,"corporation":false,"usgs":true,"family":"Capstick","given":"D.O.","email":"","affiliations":[],"preferred":false,"id":211418,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":33434,"text":"b1719E - 1987 - Mineral resources of the Owyhee Canyon Wilderness Study Area, Malheur County, Oregon","interactions":[],"lastModifiedDate":"2012-02-02T00:09:33","indexId":"b1719E","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":306,"text":"Bulletin","code":"B","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1719","chapter":"E","title":"Mineral resources of the Owyhee Canyon Wilderness Study Area, Malheur County, Oregon","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/b1719E","usgsCitation":"Evans, J.G., Hoffman, J.D., Kulik, D.M., and Linne, J.M., 1987, Mineral resources of the Owyhee Canyon Wilderness Study Area, Malheur County, Oregon: U.S. Geological Survey Bulletin 1719, v, p. E1-E18, ill., maps ;28 cm., https://doi.org/10.3133/b1719E.","productDescription":"v, p. E1-E18, ill., maps ;28 cm.","costCenters":[],"links":[{"id":166535,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1719e/report-thumb.jpg"},{"id":61317,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1719e/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b06e4b07f02db69a1c0","contributors":{"authors":[{"text":"Evans, James George","contributorId":73578,"corporation":false,"usgs":true,"family":"Evans","given":"James","email":"","middleInitial":"George","affiliations":[],"preferred":false,"id":211066,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hoffman, J. D.","contributorId":8419,"corporation":false,"usgs":true,"family":"Hoffman","given":"J.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":211063,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Kulik, D. M.","contributorId":46948,"corporation":false,"usgs":true,"family":"Kulik","given":"D.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":211064,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Linne, J. M.","contributorId":68371,"corporation":false,"usgs":true,"family":"Linne","given":"J.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":211065,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":33513,"text":"b1684 - 1987 - Petrographic and scanning electron microscope studies of samples from the Roberts Mountains and Popovich formations, Carlin Mine area, Eureka County, Nevada","interactions":[],"lastModifiedDate":"2012-02-02T00:09:41","indexId":"b1684","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":306,"text":"Bulletin","code":"B","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1684","title":"Petrographic and scanning electron microscope studies of samples from the Roberts Mountains and Popovich formations, Carlin Mine area, Eureka County, Nevada","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/b1684","usgsCitation":"Armstrong, A.K., Bagby, W., Ekburg, C., and Repetski, J., 1987, Petrographic and scanning electron microscope studies of samples from the Roberts Mountains and Popovich formations, Carlin Mine area, Eureka County, Nevada: U.S. Geological Survey Bulletin 1684, iii, 23 p. ill. (some col.), map ;28 cm., https://doi.org/10.3133/b1684.","productDescription":"iii, 23 p. ill. (some col.), map ;28 cm.","costCenters":[],"links":[{"id":165984,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1684/report-thumb.jpg"},{"id":61411,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1684/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae0e4b07f02db68804d","contributors":{"authors":[{"text":"Armstrong, Augustus K.","contributorId":68282,"corporation":false,"usgs":true,"family":"Armstrong","given":"Augustus","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":211433,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bagby, W.C.","contributorId":64663,"corporation":false,"usgs":true,"family":"Bagby","given":"W.C.","email":"","affiliations":[],"preferred":false,"id":211432,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Ekburg, Charles","contributorId":25218,"corporation":false,"usgs":true,"family":"Ekburg","given":"Charles","email":"","affiliations":[],"preferred":false,"id":211430,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Repetski, John","contributorId":60292,"corporation":false,"usgs":true,"family":"Repetski","given":"John","affiliations":[],"preferred":false,"id":211431,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":66503,"text":"i1814 - 1987 - Reconnaissance geologic map of the Noatak C5, D5, D6, and D7 quadrangles, Alaska","interactions":[{"subject":{"id":10228,"text":"ofr84396 - 1984 - Reconnaissance geologic map of the Noatak C5, D5, D6, and D7 quadrangles, Alaska","indexId":"ofr84396","publicationYear":"1984","noYear":false,"title":"Reconnaissance geologic map of the Noatak C5, D5, D6, and D7 quadrangles, Alaska"},"predicate":"SUPERSEDED_BY","object":{"id":66503,"text":"i1814 - 1987 - Reconnaissance geologic map of the Noatak C5, D5, D6, and D7 quadrangles, Alaska","indexId":"i1814","publicationYear":"1987","noYear":false,"title":"Reconnaissance geologic map of the Noatak C5, D5, D6, and D7 quadrangles, Alaska"},"id":1}],"lastModifiedDate":"2012-02-10T00:11:17","indexId":"i1814","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":320,"text":"IMAP","code":"I","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1814","subseriesTitle":"NONE","title":"Reconnaissance geologic map of the Noatak C5, D5, D6, and D7 quadrangles, Alaska","language":"ENGLISH","doi":"10.3133/i1814","usgsCitation":"Mayfield, C., Ellersieck, I., and Tailleur, I., 1987, Reconnaissance geologic map of the Noatak C5, D5, D6, and D7 quadrangles, Alaska: U.S. Geological Survey IMAP 1814, 1 map :col. ;sheet 146 x 104 cm., folded in envelope 30 x 24 cm., https://doi.org/10.3133/i1814.","productDescription":"1 map :col. ;sheet 146 x 104 cm., folded in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":107142,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_9936.htm","linkFileType":{"id":5,"text":"html"},"description":"9936"},{"id":187960,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"63360","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -165.6,67.5 ], [ -165.6,68 ], [ -164,68 ], [ -164,67.5 ], [ -165.6,67.5 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a70e4b07f02db641460","contributors":{"authors":[{"text":"Mayfield, C.F.","contributorId":95467,"corporation":false,"usgs":true,"family":"Mayfield","given":"C.F.","email":"","affiliations":[],"preferred":false,"id":274625,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ellersieck, Inyo","contributorId":34914,"corporation":false,"usgs":true,"family":"Ellersieck","given":"Inyo","affiliations":[],"preferred":false,"id":274623,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Tailleur, I.L.","contributorId":59027,"corporation":false,"usgs":true,"family":"Tailleur","given":"I.L.","email":"","affiliations":[],"preferred":false,"id":274624,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":33522,"text":"b1696 - 1987 - Multispectral Landsat images of Antarctica","interactions":[],"lastModifiedDate":"2018-10-31T15:34:14","indexId":"b1696","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":306,"text":"Bulletin","code":"B","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1696","title":"Multispectral Landsat images of Antarctica","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey,","doi":"10.3133/b1696","usgsCitation":"Lucchitta, B.K., Bowell, J., Edwards, K., Eliason, E.M., and Ferguson, H., 1987, Multispectral Landsat images of Antarctica: U.S. Geological Survey Bulletin 1696, iii, 21 p. ill. (chiefly col.), map ;28 cm., https://doi.org/10.3133/b1696.","productDescription":"iii, 21 p. ill. (chiefly col.), map ;28 cm.","costCenters":[{"id":131,"text":"Astrogeology Science Center","active":true,"usgs":true}],"links":[{"id":61425,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1696/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":166600,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1696/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b32e4b07f02db6b48c8","contributors":{"authors":[{"text":"Lucchitta, Baerbel K. blucchitta@usgs.gov","contributorId":3649,"corporation":false,"usgs":true,"family":"Lucchitta","given":"Baerbel","email":"blucchitta@usgs.gov","middleInitial":"K.","affiliations":[],"preferred":true,"id":211445,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bowell, Jo-Ann","contributorId":103722,"corporation":false,"usgs":true,"family":"Bowell","given":"Jo-Ann","email":"","affiliations":[],"preferred":false,"id":211449,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Edwards, K.L.","contributorId":53864,"corporation":false,"usgs":true,"family":"Edwards","given":"K.L.","email":"","affiliations":[],"preferred":false,"id":211446,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Eliason, E. M.","contributorId":93113,"corporation":false,"usgs":true,"family":"Eliason","given":"E.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":211448,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Ferguson, H.M.","contributorId":61083,"corporation":false,"usgs":true,"family":"Ferguson","given":"H.M.","email":"","affiliations":[],"preferred":false,"id":211447,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":34970,"text":"b1779 - 1987 - Regional thermal metamorphism and deformation of the Sitka Graywacke, southern Baranof Island, southeastern Alaska","interactions":[],"lastModifiedDate":"2012-02-02T00:09:41","indexId":"b1779","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":306,"text":"Bulletin","code":"B","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1779","title":"Regional thermal metamorphism and deformation of the Sitka Graywacke, southern Baranof Island, southeastern Alaska","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/b1779","usgsCitation":"Loney, R.A., and Brew, D.A., 1987, Regional thermal metamorphism and deformation of the Sitka Graywacke, southern Baranof Island, southeastern Alaska: U.S. Geological Survey Bulletin 1779, iii, 17 p. ill., maps ;28 cm., https://doi.org/10.3133/b1779.","productDescription":"iii, 17 p. ill., maps ;28 cm.","costCenters":[],"links":[{"id":167080,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1779/report-thumb.jpg"},{"id":62918,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1779/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a60e4b07f02db634e5d","contributors":{"authors":[{"text":"Loney, Robert Ahlberg","contributorId":72802,"corporation":false,"usgs":true,"family":"Loney","given":"Robert","email":"","middleInitial":"Ahlberg","affiliations":[],"preferred":false,"id":213910,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Brew, David A. dbrew@usgs.gov","contributorId":3244,"corporation":false,"usgs":true,"family":"Brew","given":"David","email":"dbrew@usgs.gov","middleInitial":"A.","affiliations":[],"preferred":true,"id":213909,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":60977,"text":"mf1974 - 1987 - Seismicity map of the state of Indiana","interactions":[{"subject":{"id":60978,"text":"mf1145 - 1979 - Seismicity map of the State of Indiana","indexId":"mf1145","publicationYear":"1979","noYear":false,"title":"Seismicity map of the State of Indiana"},"predicate":"SUPERSEDED_BY","object":{"id":60977,"text":"mf1974 - 1987 - Seismicity map of the state of Indiana","indexId":"mf1974","publicationYear":"1987","noYear":false,"title":"Seismicity map of the state of Indiana"},"id":1}],"lastModifiedDate":"2025-05-27T16:36:24.580801","indexId":"mf1974","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":325,"text":"Miscellaneous Field Studies Map","code":"MF","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1974","title":"Seismicity map of the state of Indiana","docAbstract":"<p>This map is one of a series of seismicity maps produced by the U. S. Geological Survey that show earthquake data of individual states or groups of states at the scale of 1:1,000,000. This map shows only those earthquakes with epicenters located within the boundaries of Indiana, even though earthquakes in nearby states may have been felt or may have caused damage in Indiana.</p>\n<p>The data in table 1 were used to compile the seismicity map; these data are a corrected, expanded, and updated (through 1983) version of the data used by Algermissen (1969) for a study of seismic risk in the United States. The locations and intensities of some earthquakes were revised and intensities were assigned where none had been before. Many earthquakes were added to the original list from new data sources as well as from some old data sources that had not been previously used. The data in table 1 represent best estimates of the location of the epicenter, magnitude, and intensity of each earthquake on the basis of historical and current information. Some of the aftershocks from large earthquakes are listed, but not all, especially for earthquakes that occurred before seismic instruments were universally used.</p>\n<p>The latitude and longitude coordinates of each epicenter were rounded to the nearest tenth of a degree and sorted so that all identical locations were grouped and counted. These locations are represented on the map by a triangle. The number of earthquakes at each location is shown on the map by the arabic number to the right of the triangle. A Roman numeral to the left of a triangle is the maximum Modified Mercalli intensity (Wood and Neumann, 1931) of all earthquakes at that geographic location. The absence of an intensity value indicates that no intensities have been assigned to earthquakes at that location. The year shown below each triangle is the latest year for which the maximum intensity was recorded.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/mf1974","usgsCitation":"Stover, C.W., Reagor, B., and Algermissen, S.T., 1987, Seismicity map of the state of Indiana (Supercedes MF-1145): U.S. Geological Survey Miscellaneous Field Studies Map 1974, 1 Plate: 36.57 x 22.18 inches, https://doi.org/10.3133/mf1974.","productDescription":"1 Plate: 36.57 x 22.18 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":180557,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/mf1974.PNG"},{"id":486594,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_5545.htm","linkFileType":{"id":5,"text":"html"}},{"id":327538,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1974/plate-1.pdf","size":"7.47 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